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âmbar

Amber is fossilized tree resin that has hardened over millions of years. It forms when resin escapes from ancient trees, is buried and preserved, and undergoes polymerization and dehydration to become durable stone. The result is a hard, often translucent material that can range in color from pale yellow to deep orange or brown.

Amber commonly occurs with inclusions, such as trapped insects, plant fragments, or air bubbles. These inclusions

Geologically, the best-known amber comes from the Baltic region and is often referred to as succinite. Other

Historically and culturally, amber has been used for jewelry, carvings, and decorative objects since ancient times.

Distinguishing amber from younger resins such as copal and from synthetic resins often requires closer examination,

preserve
microscopic
details
and
provide
valuable
information
about
ancient
ecosystems,
climates,
and
environments.
important
sources
include
the
Dominican
Republic,
Myanmar
(Burmese
amber),
and
Mexico.
The
age
of
amber
varies
by
deposit,
with
Baltic
amber
dating
to
the
Eocene
and
other
deposits
spanning
from
the
Cretaceous
to
the
Miocene.
It
also
yielded
succinic
acid,
which
was
once
used
in
medicine
and
industry.
Today,
amber
remains
prized
for
its
beauty
and
its
scientific
value,
particularly
for
the
study
of
prehistoric
life
through
inclusions.
including
microscopic
analysis
of
inclusions,
color,
and
fluorescence
under
light.
Amber’s
appearance
and
provenance—together
with
characteristic
inclusions—help
determine
its
origin
and
age.